Relationship between probable dominant phosphate compound in soil and phosphorus availability to plants

Summary Surface soil materials from the 0- to 15 cm depth of 12 sites that were suspected to contain high levels of P, as a result of years of repeated applications of either inorganic or organic P fertilizers, were cropped with wheat and alfalfa in the greenhouse for about one year. The total P removed in plant materials provided an estimate of the plant available P in the soils. The probable dominant phosphate compound controlling the release of P in the soil solution during cropping was determined using the GEOCHEM program and an activity diagram. The data show that P availability is partly dependent on the stability of the phosphate compound present, although the relative positions of the points on the activity diagram show no quantitative relationship with either the total plant P uptake or the phosphate buffering capacity of the soils. The positions of the points, however, indicate that with time the formation of more stable P compounds during cropping could be attributed to reactions in the soil as well as to crop removal. The more soluble compounds could have recrystallized or were transformed into compounds of lower solubility. There is also the possibility that the more soluble P compounds were exhausted by crop removal leaving behind the less soluble compounds.